Jörg Ebbing

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The Gravity field and steady-state Ocean Circulation Explorer (GOCE) satellite aimed at determining the Earth's mean gravity field. GOCE delivered gravity gradients containing directional information, which are complicated to use because of their error characteristics and because they are given in a rotating instrument frame indirectly related to the Earth.(More)
Key Points: • The GIA free-air anomaly cannot be retrieved from the static gravity field • Numerical GIA models are accurate enough to correct the gravity field • The GIA gravity signal is sensitive to the asthenosphere density (2015), Glacial isostatic adjustment in the static gravity field of Fennoscandia, Abstract In the central part of Fennoscandia, the(More)
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